Geological characteristics of neoproterozoic motianling granitic pluton hosting uranium mineralization in North Guangxi, China: Insights from biotite chemistry Article Swipe
Peng Luo
,
Guo Chunying
,
Qiaohui Pi
,
Ning Wang
,
Naiyuan Liu
·
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.3389/feart.2025.1558551
YOU?
·
· 2025
· Open Access
·
· DOI: https://doi.org/10.3389/feart.2025.1558551
The Motianling pluton represents a characteristic U-bearing granite pluton in South China. Biotite serves as an indicator for the mineralization of metals such as Cu, Sn, and W in granite. Previous studies have extensively investigated the U metallogenic potential of the Motianling pluton, but research on the indicative role of biotite geochemistry in U mineralization remains limited. This study selected biotite from the coarse-grained and medium-grained granites of the Motianling pluton as the research subject. Utilizing optical microscopy, electron probe microanalysis (EPMA), and other techniques, a petrographic and geochemical study was conducted, supplemented by a comprehensive analysis of the geochemical data of biotite from typical U-bearing granites in South China. The analytical results reveal that the biotite in the coarse-grained granite is Fe-biotite (FeO t : 22.88 to 26.15 wt%, Al 2 O 3 : 16.62 to 17.76 wt%, MgO: 4.52 to 6.99 wt%, TiO 2 : 1.37 to 3.04 wt%), while in the medium-grained granite, it is siderophyllite (FeO t : 27.96 to 30.02 wt%, Al 2 O 3 : 17.78 to 18.50 wt%, MgO: 1.41 to 2.01 wt%, TiO 2 : 1.43 to 2.03 wt%). Additionally, the biotite in the mediumgrained granite exhibits higher concentrations of Fe and Al but lower levels of Mg and Ti compared to the coarsegrained granite. The geochemical characteristics of biotite indicate that the Motianling granite is S-type granite, characterized by relatively low temperature and low oxygen fugacity ( f O2 ). The geochemical properties of biotite have certain indicative significance for U enrichment. Biotite from the medium-grained granite exhibits higher U concentrations, a lower Th/U ratio, and lower crystallization temperatures and oxygen fugacity relative to the coarsegrained granite, suggesting enhanced U mineralization potential in the medium-grained granite.
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- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.3389/feart.2025.1558551
- https://www.frontiersin.org/journals/earth-science/articles/10.3389/feart.2025.1558551/pdf
- OA Status
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- References
- 51
- Related Works
- 10
- OpenAlex ID
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- OpenAlex ID
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https://openalex.org/W4409892888Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.3389/feart.2025.1558551Digital Object Identifier
- Title
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Geological characteristics of neoproterozoic motianling granitic pluton hosting uranium mineralization in North Guangxi, China: Insights from biotite chemistryWork title
- Type
-
articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2025Year of publication
- Publication date
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2025-04-28Full publication date if available
- Authors
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Peng Luo, Guo Chunying, Qiaohui Pi, Ning Wang, Naiyuan LiuList of authors in order
- Landing page
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https://doi.org/10.3389/feart.2025.1558551Publisher landing page
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https://www.frontiersin.org/journals/earth-science/articles/10.3389/feart.2025.1558551/pdfDirect link to full text PDF
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goldOpen access status per OpenAlex
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https://www.frontiersin.org/journals/earth-science/articles/10.3389/feart.2025.1558551/pdfDirect OA link when available
- Concepts
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Pluton, Biotite, Geology, Geochemistry, Mineralization (soil science), Uranium, China, Tectonics, Soil science, Seismology, Soil water, Materials science, Quartz, Metallurgy, Law, Paleontology, Political scienceTop concepts (fields/topics) attached by OpenAlex
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0Total citation count in OpenAlex
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51Number of works referenced by this work
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10Other works algorithmically related by OpenAlex
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| abstract_inverted_index.Fe | 198 |
| abstract_inverted_index.Mg | 205 |
| abstract_inverted_index.O2 | 237 |
| abstract_inverted_index.Ti | 207 |
| abstract_inverted_index.an | 15 |
| abstract_inverted_index.as | 14, 23, 71 |
| abstract_inverted_index.by | 93, 227 |
| abstract_inverted_index.in | 9, 28, 52, 107, 117, 152, 190, 281 |
| abstract_inverted_index.is | 121, 157, 223 |
| abstract_inverted_index.it | 156 |
| abstract_inverted_index.of | 20, 39, 49, 67, 97, 101, 197, 204, 216, 242 |
| abstract_inverted_index.on | 45 |
| abstract_inverted_index.to | 127, 136, 141, 148, 163, 172, 177, 184, 209, 272 |
| abstract_inverted_index.Cu, | 24 |
| abstract_inverted_index.Sn, | 25 |
| abstract_inverted_index.The | 0, 110, 213, 239 |
| abstract_inverted_index.TiO | 144, 180 |
| abstract_inverted_index.and | 26, 64, 82, 87, 199, 206, 231, 264, 268 |
| abstract_inverted_index.but | 43, 201 |
| abstract_inverted_index.for | 17, 248 |
| abstract_inverted_index.low | 229, 232 |
| abstract_inverted_index.the | 18, 35, 40, 46, 62, 68, 72, 98, 115, 118, 153, 188, 191, 210, 220, 253, 273, 282 |
| abstract_inverted_index.was | 90 |
| abstract_inverted_index.(FeO | 123, 159 |
| abstract_inverted_index.1.37 | 147 |
| abstract_inverted_index.1.41 | 176 |
| abstract_inverted_index.1.43 | 183 |
| abstract_inverted_index.2.01 | 178 |
| abstract_inverted_index.2.03 | 185 |
| abstract_inverted_index.3.04 | 149 |
| abstract_inverted_index.4.52 | 140 |
| abstract_inverted_index.6.99 | 142 |
| abstract_inverted_index.MgO: | 139, 175 |
| abstract_inverted_index.Th/U | 262 |
| abstract_inverted_index.This | 57 |
| abstract_inverted_index.data | 100 |
| abstract_inverted_index.from | 61, 103, 252 |
| abstract_inverted_index.have | 32, 244 |
| abstract_inverted_index.role | 48 |
| abstract_inverted_index.such | 22 |
| abstract_inverted_index.that | 114, 219 |
| abstract_inverted_index.wt%, | 129, 138, 143, 165, 174, 179 |
| abstract_inverted_index.16.62 | 135 |
| abstract_inverted_index.17.76 | 137 |
| abstract_inverted_index.17.78 | 171 |
| abstract_inverted_index.18.50 | 173 |
| abstract_inverted_index.22.88 | 126 |
| abstract_inverted_index.26.15 | 128 |
| abstract_inverted_index.27.96 | 162 |
| abstract_inverted_index.30.02 | 164 |
| abstract_inverted_index.South | 10, 108 |
| abstract_inverted_index.lower | 202, 261, 265 |
| abstract_inverted_index.other | 83 |
| abstract_inverted_index.probe | 79 |
| abstract_inverted_index.study | 58, 89 |
| abstract_inverted_index.while | 151 |
| abstract_inverted_index.wt%), | 150 |
| abstract_inverted_index.wt%). | 186 |
| abstract_inverted_index.China. | 11, 109 |
| abstract_inverted_index.S-type | 224 |
| abstract_inverted_index.higher | 195, 257 |
| abstract_inverted_index.levels | 203 |
| abstract_inverted_index.metals | 21 |
| abstract_inverted_index.oxygen | 233, 269 |
| abstract_inverted_index.pluton | 2, 8, 70 |
| abstract_inverted_index.ratio, | 263 |
| abstract_inverted_index.reveal | 113 |
| abstract_inverted_index.serves | 13 |
| abstract_inverted_index.(EPMA), | 81 |
| abstract_inverted_index.Biotite | 12, 251 |
| abstract_inverted_index.biotite | 50, 60, 102, 116, 189, 217, 243 |
| abstract_inverted_index.certain | 245 |
| abstract_inverted_index.granite | 7, 120, 193, 222, 255 |
| abstract_inverted_index.optical | 76 |
| abstract_inverted_index.pluton, | 42 |
| abstract_inverted_index.remains | 55 |
| abstract_inverted_index.results | 112 |
| abstract_inverted_index.studies | 31 |
| abstract_inverted_index.typical | 104 |
| abstract_inverted_index.Previous | 30 |
| abstract_inverted_index.analysis | 96 |
| abstract_inverted_index.compared | 208 |
| abstract_inverted_index.electron | 78 |
| abstract_inverted_index.enhanced | 277 |
| abstract_inverted_index.exhibits | 194, 256 |
| abstract_inverted_index.fugacity | 234, 270 |
| abstract_inverted_index.granite, | 155, 225, 275 |
| abstract_inverted_index.granite. | 29, 212, 284 |
| abstract_inverted_index.granites | 66, 106 |
| abstract_inverted_index.indicate | 218 |
| abstract_inverted_index.limited. | 56 |
| abstract_inverted_index.relative | 271 |
| abstract_inverted_index.research | 44, 73 |
| abstract_inverted_index.selected | 59 |
| abstract_inverted_index.subject. | 74 |
| abstract_inverted_index.U-bearing | 6, 105 |
| abstract_inverted_index.Utilizing | 75 |
| abstract_inverted_index.indicator | 16 |
| abstract_inverted_index.potential | 38, 280 |
| abstract_inverted_index.Fe-biotite | 122 |
| abstract_inverted_index.Motianling | 1, 41, 69, 221 |
| abstract_inverted_index.analytical | 111 |
| abstract_inverted_index.conducted, | 91 |
| abstract_inverted_index.indicative | 47, 246 |
| abstract_inverted_index.properties | 241 |
| abstract_inverted_index.relatively | 228 |
| abstract_inverted_index.represents | 3 |
| abstract_inverted_index.suggesting | 276 |
| abstract_inverted_index.enrichment. | 250 |
| abstract_inverted_index.extensively | 33 |
| abstract_inverted_index.geochemical | 88, 99, 214, 240 |
| abstract_inverted_index.microscopy, | 77 |
| abstract_inverted_index.techniques, | 84 |
| abstract_inverted_index.temperature | 230 |
| abstract_inverted_index.geochemistry | 51 |
| abstract_inverted_index.investigated | 34 |
| abstract_inverted_index.metallogenic | 37 |
| abstract_inverted_index.petrographic | 86 |
| abstract_inverted_index.significance | 247 |
| abstract_inverted_index.supplemented | 92 |
| abstract_inverted_index.temperatures | 267 |
| abstract_inverted_index.Additionally, | 187 |
| abstract_inverted_index.characterized | 226 |
| abstract_inverted_index.coarsegrained | 211, 274 |
| abstract_inverted_index.comprehensive | 95 |
| abstract_inverted_index.mediumgrained | 192 |
| abstract_inverted_index.microanalysis | 80 |
| abstract_inverted_index.characteristic | 5 |
| abstract_inverted_index.coarse-grained | 63, 119 |
| abstract_inverted_index.concentrations | 196 |
| abstract_inverted_index.medium-grained | 65, 154, 254, 283 |
| abstract_inverted_index.mineralization | 19, 54, 279 |
| abstract_inverted_index.siderophyllite | 158 |
| abstract_inverted_index.characteristics | 215 |
| abstract_inverted_index.concentrations, | 259 |
| abstract_inverted_index.crystallization | 266 |
| cited_by_percentile_year | |
| countries_distinct_count | 0 |
| institutions_distinct_count | 5 |
| citation_normalized_percentile.value | 0.19189399 |
| citation_normalized_percentile.is_in_top_1_percent | False |
| citation_normalized_percentile.is_in_top_10_percent | False |